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New groundwater-level rise data from the Rhine-Meuse delta – implications for the reconstruction of Holocene relative mean sea-level rise and differential land-level movements

Published online by Cambridge University Press:  01 April 2016

H.J.A. Berendsen ,
B Makaske ,
O. van de Plassche ,
M.H.M van Ree ,
S. Das ,
M. van Dongen ,
S. Ploumen  and
W. Schoenmakers
H.J.A. Berendsen
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
B Makaske*
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, the Netherlands; now at: Alterra, Wageningen University and Research Centre, P.O. Box 47, 6700 AA Wageningen, the Netherlands
O. van de Plassche
Affiliation:
Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands.
M.H.M van Ree
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
S. Das
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
M. van Dongen
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
S. Ploumen
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
W. Schoenmakers
Affiliation:
Faculty of Geosciences, Department of Physical Geography, Utrecht University, Heidelberglaan 2, 3534 CS Utrecht, the Netherlands
*
* Corresponding author. Email: [email protected]
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Abstract

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We present new local groundwater-level rise data from two Late Glacial aeolian dunes, located near Barendrecht and Oud-Alblas in the western Rhine-Meuse delta. These data are based on AMS radiocarbon dating of terrestrial macrofossils, collected from the base of peat formed on the slopes of these dunes. This method avoids contamination of bulk peat samples by old soil carbon or younger rootlets and rhizomes, as well as the hardwater effect. The new data are used to assess the reliability of previously published groundwater-level index data based on conventional radiocarbon dating of bulk basal peat samples from the slopes of the Late Glacial aeolian dunes at Barendrecht, Hillegersberg, Bolnes and Wijngaarden, all located in the western Rhine-Meuse delta.

Comparison of the new and published groundwater-level data shows no significant systematic difference between conventionally dated bulk peat samples and AMS-dated samples of terrestrial macrofossils. The new data from the dune at Barendrecht confirm the reliability of the younger than 6600 cal yr BP age-depth data from the dunes at Hillegersberg and near Bolnes. This result supports the validity of this part of the mean sea-level (MSL) curve for the western Netherlands. Consequently, the position of the groundwater-level curve for Flevoland (central Netherlands) below this MSL curve can most likely be attributed to differential land-level movement.

The available data show that the groundwater-gradient effect in the western Rhine-Meuse delta became less than 5 cm/km after 6600 cal yr BP. Finally, temporal correlation between temporary increases in local groundwater-level rise with known shifts of river courses in the delta plain suggests, that avulsions can explain sudden local deviations from the trend in groundwater-level rise. A general conclusion of this study is that a complex relationship exists between sea level and local delta-plain water levels.

Keywords

AMS datingavulsionsHolocene sea-level riseLate Glacial aeolian dunesriver-gradient effect
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 86 , Issue 4 , December 2007 , pp. 333 - 354
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2007

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